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Bloke Plateau
The Bloke Plateau ( sl, Bloška planota, Bloke) is an extensive bowl-like plateau in southwest Slovenia, part of the traditional region of Inner Carniola. Geography The Bloke Plateau measures approximately long and wide. It ranges in elevation between and . Together with the Rakitna tectonic block, the plateau is delineated by two distinct Dinaric faults. According to the geographer Anton Melik, the Bloke Plateau is a remnant of a Pliocene peneplain in the middle of the rejuvenated terrain. Poorly permeable karst limestone and Triassic dolomite (in the northern part of the plateau) conditioned the formation of typical surface watercourses (Bloščica Creek and Blatnica Creek), which are bounded by wet grasslands and minerotrophic fens. Lake Bloke ( sl, Bloško jezero), a reservoir, lies near the settlement of Volčje. Water flows below ground from the Bloke Plateau into Lake Cerknica. The plateau's many hills divide it into the Bloščica Valley and Ločica Valley (or Farovšč ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nova Vas, Bloke
Nova Vas (; sl, Nova vas, german: Neudorf) is the largest village and the administrative centre of the Municipality of Bloke in the Inner Carniola region of Slovenia Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, an .... Name Nova Vas was attested in written sources as ''villa nova'' in 1282, ''Newndorf'' in 1341, and ''Newdarff'' in 1499, among other spellings. The name ''Nova vas'' literally means 'new village', designating a settlement that was created later than nearby villages. ''Nova vas'' is a common toponym in Slovenia. References External links *Nova Vas on Geopedia Populated places in the Municipality of Bloke {{Bloke-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Fields
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Plateaus Of Slovenia
Karst is a topography formed from the dissolution of soluble rocks such as limestone, Dolomite (rock), dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German language, German in the late 19th century, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Croatia
, image_flag = Flag of Croatia.svg , image_coat = Coat of arms of Croatia.svg , anthem = "Lijepa naša domovino"("Our Beautiful Homeland") , image_map = , map_caption = , capital = Zagreb , coordinates = , largest_city = capital , official_languages = Croatian , languages_type = Writing system , languages = Latin , ethnic_groups = , ethnic_groups_year = 2021 , religion = , religion_year = 2021 , demonym = , government_type = Unitary parliamentary republic , leader_title1 = President , leader_name1 = Zoran Milanović , leader_title2 = Prime Minister , leader_name2 = Andrej Plenković , leader_title3 = Speaker of Parliament , leader_name3 = Gordan Jandroković , legislature = Sabor , sovereignty_type ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lower Carniola
Lower Carniola ( sl, Dolenjska; german: Unterkrain) is a traditional region in Slovenia, the southeastern part of the historical Carniola region. Geography Lower Carniola is delineated by the Ljubljana Basin with the city of Ljubljana to the northwest, by the Kolpa River and the border with Croatia with the Gorjanci Mountains to the south and southeast, by the Sava River to the north and northeast, and by Mount Krim, the Bloke Plateau, and the Potok Plateau ( sl, Potočanska planota) to the west. The southernmost region down to the border with Croatia on the Kolpa River is called White Carniola and usually considered part of Lower Carniola. Within the Kočevje Rog karst plateau, the mountains reach an elevation of up to . The historic centre of Lower Carniola is Novo Mesto, and other towns include Kočevje, Grosuplje, Krško, Trebnje, Mirna, Črnomelj, Semič, and Metlika. History In the 17th century, the Habsburg duchy of Carniola was internally divided into three admi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carniola
Carniola ( sl, Kranjska; , german: Krain; it, Carniola; hu, Krajna) is a historical region that comprised parts of present-day Slovenia. Although as a whole it does not exist anymore, Slovenes living within the former borders of the region still tend to identify with its traditional parts Upper Carniola, Lower Carniola (with the sub-part of White Carniola), and to a lesser degree with Inner Carniola. In 1991, 47% of the population of Slovenia lived within the borders of the former Duchy of Carniola. Overview A state of the Holy Roman Empire in the Austrian Circle and a duchy in the hereditary possession of the Habsburgs, later part of the Austrian Empire and of Austria-Hungary, the region was a crown land from 1849, when it was also subdivided into Upper Carniola, Lower Carniola, and Inner Carniola, until 1918. From the second half of the 13th century, its capital was Ljubljana (Laibach). Previous overlords of Carniola had their seats in Kranj (Krainburg) and Kamnik (Stein), wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Benete
Benete () is a small settlement in the hills east of Nova Vas in the Municipality of Bloke in the Inner Carniola region of Slovenia Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, an .... References External links Benete on Geopedia Populated places in the Municipality of Bloke {{Bloke-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pannonian Basin
The Pannonian Basin, or Carpathian Basin, is a large Sedimentary basin, basin situated in south-east Central Europe. The Geomorphology, geomorphological term Pannonian Plain is more widely used for roughly the same region though with a somewhat different sense, with only the Upland and lowland, lowlands, the plain that remained when the Pliocene Epoch ''Pannonian Sea'' dried out. It is a geomorphological subsystem of the Alpide belt, Alps-Himalaya system, specifically a sediment-filled back-arc basin which divergent boundary, spread apart during the Miocene. The plain or basin is diagonally bisected by the Transdanubian Mountains, separating the larger Great Hungarian Plain (including the Eastern Slovak Lowland) from the Little Hungarian Plain. It forms a topographically discrete unit set in the European landscape, surrounded by imposing geographic boundaries—the Carpathian Mountains and the Alps. The Rivers Danube and Tisza divide the basin roughly in half. It extends rough ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kvarner Gulf
The Kvarner Gulf (, or , la, Sinus Flanaticus or ), sometimes also Kvarner Bay, is a bay in the northern Adriatic Sea, located between the Istrian peninsula and the northern Croatian Littoral mainland. The bay is a part of Croatia's internal waters. The largest islands within the Kvarner are Cres, Krk, Pag, Rab and Lošinj. A portion of the Kvarner Bay, located between Cres, Krk, Rab and Pag is also called ''Kvarnerić'' (literally "little Kvarner") or or , and the portion east of Krk and Rab is called Senj Channel. The bay is notable for its depth (more than 100 meters), which allows for the city of Rijeka at its northernmost point to have a sea port that can accommodate Capesize ships. The bay is also home to many beaches and tourist locations because of its beautiful waters and warm climate. See also * Geography of Croatia The geography of Croatia is defined by its location—it is described as a part of Central Europe and Southeast Europe, a part of the Balkans an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aquileia
Aquileia / / / / ;Bilingual name of ''Aquileja – Oglej'' in: vec, Aquiłeja / ; Slovenian: ''Oglej''), group=pron is an ancient Roman city in Italy, at the head of the Adriatic at the edge of the lagoons, about from the sea, on the river Natiso (modern Natisone), the course of which has changed somewhat since Roman times. Today, the city is small (about 3,500 inhabitants), but it was large and prominent in classical antiquity as one of the world's largest cities with a population of 100,000 in the 2nd century AD and is one of the main archaeological sites of northern Italy. In late antiquity the city was the first city in the Italian Peninsula to be sacked by Attila the Hun. History Classical Antiquity Roman Republic Aquileia was founded as a colony by the Romans in 180/181 BC along the Natiso River, on land south of the Julian Alps but about north of the lagoons. The colony served as a strategic frontier fortress at the north-east corner of transpadane Ital ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iapydes
The Iapydes (or Iapodes, Japodes; el, Ἰάποδες) were an ancient people who dwelt north of and inland from the Liburnians, off the Adriatic coast and eastwards of the Istrian peninsula. They occupied the interior of the country between the ''Colapis'' (Kupa) and ''Oeneus'' (Una) rivers, and the Velebit mountain range (''Mons Baebius'') which separated them from the coastal Liburnians. Their territory covered the central inlands of modern Croatia and Una River Valley in today's Bosnia and Herzegovina. Archaeological documentation confirms their presence in these countries at least from 9th century BC, and they persisted in their area longer than a millennium. The ancient written documentation on inland Iapydes is scarcer than on the adjacent coastal peoples (Liburni, Delmatae, etc.) that had more frequent maritime contacts with ancient Greeks and Romans. The Iapydes had their maximal development and territorial expansion from the 8th to 4th centuries BC. They settled mostly i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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